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石油与天然气地质 第6期 oL GAS gEology 005年12月 文章编号:0253.9985(2005)06-0724.06 我国典型天然气藏输导体系研究 以鄂尔多斯盆地苏里格气田为例 朱筱敏刘成林,曾庆猛2门相勇 (1中国石油大学,北京10249,2中国地质大学北京100083 3中国石油勘探开发研究院,北京100083) 摘要:前陆盆地褶皱·冲断带气藏和裂谷盆地气藏油气输导体系以断裂为主,天然气运移方向以垂向为主,运移距离短,输 导效率高;而克拉通盆地岩性气藏和前陆盆地斜坡带气藏油气输导体系以砂体为主,油气运移方向为侧向、垂向,运移距 离较长,输导效率低。苏里格气田属克拉通盆地岩性气藏输导体系主要类型为砂体型,也有少量断裂型、砂体-断裂型 砂体型又可进一步分为厚层带状砂体、薄层带状砂体与透镜状砂体等类型。输导体系的输导能力随时间而变化。在 200~150M溶蚀作用和断层活动最强,输导体系的输导能力增大到顶峰。在成藏关键时刻(J3一K)输导体系格架产状 西高东低、北高南低,主要输导体系为砂体、断层与裂缝,油气向西北方向运移,输导效率高。在成藏后调整期(K-Q) 输导体系格架大部为东高西低、北高南低,主要输导体系为砂体与裂缝。油气运移效率较低,运移不太明显 关键词输导体系;克拉通;前陆;裂谷;苏里格气田;鄂尔多斯盆地 中图分类号:TE1121 文献标 Study of carrier system of typ ica l gas reservo irs in China taking Sulige gas field in O rdos basin as an examp le Zhu X iaom n, L iu Chenglin, Zeng Q ingmeng, Men Xiangyu 3 Research Institute of Petroleun Exploration and Developm ent PetroChina, Beijing) Abstract: For gas re servoirs in the fold-thrust belts of fore land basins and in rift basins, faults constitu te the main carrier systems, and hydrocarbons m grate mainly in vertical directin with short m igraton distance and high delivery effic iency While for litho bogic gas reservoirs in craton basins and gas reservoirs in sbpe zones of foreland basins, sandbod ies act as the main carrier system, and hyd rocarbonsm grate both laterally and vertical- ly with re latively bng m igration distance and bw delivery efficiency. Sulige gas field is of litho bgic gas reser voirs in cratn basin, its main carrier system is of sandbody type, with a few fault type and sandbody-fault type carrier systems The sandbody carrier system can be subdivided inb thick belt sandbody, thin belt sandbody and lenticular sandbody. The delivery capacity of carrier system varied with tme It peaked in 200-150 Ma during the strongest disso lutin and faulting At the critical reservoiring perod(J3-K), the framework of car rier system was high in the west and north and bw in the east and south, and the mapr carrier system consisted of sandbodies, faults and frac tures Hydrocarbons m igra ted northwestard with high de livery effic iency While in the post-re servoiring ad jusment period(K-Q), the framework of carrier system was basically high in the east and north and low in the west and south, and the major carrier system consisted of sandbody and frac tures Hydrocarbon m igraton effic iency was bw and not evident Key words: carrier systam: cran, foreland; rift Sulige gas field; O rdos basin 基金项目国家重点基础研究发展规划(973)项目(2001CB209103) 第一作者简介:朱筱敏,男,45岁,教授,石油地质与沉积储层 收稿日期:2005-09-27 2 01994-2007 China Academic Journal Electronie Publishing House. All rights reserved. hup: /wwe cnki net石油与天然气地质 第 26卷 第 6期 O IL & GAS GEOLOGY 2005年 12月 基金项目 :国家重点基础研究发展规划 (973)项目 (2001CB209103) 第一作者简介 :朱筱敏 ,男 , 45岁 ,教授 ,石油地质与沉积储层 收稿日期 : 2005 - 09- 27 文章编号 : 0253 - 9985 (2005) 06 - 0724 - 06 我国典型天然气藏输导体系研究 ———以鄂尔多斯盆地苏里格气田为例 朱筱敏 1 ,刘成林 1 ,曾庆猛 2 ,门相勇 3 (1. 中国石油大学 , 北京 102249; 2. 中国地质大学 ,北京 100083; 3. 中国石油勘探开发研究院 ,北京 100083) 摘要 :前陆盆地褶皱 - 冲断带气藏和裂谷盆地气藏油气输导体系以断裂为主 ,天然气运移方向以垂向为主 ,运移距离短 ,输 导效率高 ;而克拉通盆地岩性气藏和前陆盆地斜坡带气藏油气输导体系以砂体为主 ,油气运移方向为侧向、垂向 ,运移距 离较长 ,输导效率低。苏里格气田属克拉通盆地岩性气藏 ,输导体系主要类型为砂体型 ,也有少量断裂型、砂体 - 断裂型。 砂体型又可进一步分为厚层带状砂体、薄层带状砂体与透镜状砂体等类型。输导体系的输导能力随时间而变化。在 200~150Ma溶蚀作用和断层活动最强 ,输导体系的输导能力增大到顶峰。在成藏关键时刻 (J3 —K1 ) ,输导体系格架产状 西高东低、北高南低 ,主要输导体系为砂体、断层与裂缝 ,油气向西北方向运移 ,输导效率高。在成藏后调整期 ( K2 —Q) , 输导体系格架大部为东高西低、北高南低 ,主要输导体系为砂体与裂缝。油气运移效率较低 ,运移不太明显。 关键词 :输导体系 ;克拉通 ;前陆 ;裂谷 ;苏里格气田 ;鄂尔多斯盆地 中图分类号 : TE112. 1 文献标识码 : A Study of carr ier system of typica l ga s reservo irs in China —taking Sulige gas field in O rdos basin as an examp le Zhu Xiaom in 1 ,L iu Chenglin 1 , Zeng Q ingmeng 2 ,Men Xiangyong 3 (1. China University of Petroleum , B eijing; 2. China University of Geosciences, B eijing; 3. Research Institute of Petroleum Exploration and Developm ent, PetroChina, B eijing) Abstract:For gas reservoirs in the fold2thrust belts of foreland basins and in rift basins, faults constitute the main carrier system s, and hydrocarbons m igrate mainly in vertical direction with short m igration distance and high delivery efficiency. W hile for lithologic gas reservoirs in craton basins and gas reservoirs in slope zones of foreland basins, sandbodies act as the main carrier system, and hydrocarbonsm igrate both laterally and vertical2 ly with relatively long m igration distance and low delivery efficiency. Sulige gas field is of lithologic gas reser2 voirs in craton basin, itsmain carrier system is of sandbody type, with a few fault type and sandbody2fault type carrier system s. The sandbody carrier system can be subdivided into thick belt sandbody, thin belt sandbody and lenticular sandbody. The delivery capacity of carrier system varied with time. It peaked in 200 - 150 Ma during the strongest dissolution and faulting. A t the critical reservoiring period (J3 - K1 ) , the framework of car2 rier system was high in the west and north and low in the east and south, and the major carrier system consisted of sandbodies, faults and fractures. Hydrocarbons m igrated northwestward with high delivery efficiency. W hile in the post2reservoiring adjustment period ( K2 - Q) , the framework of carrier system was basically high in the east and north and low in the west and south, and the major carrier system consisted of sandbody and fractures. Hydrocarbon m igration efficiency was low and not evident. Key words: carrier system; craton; foreland; rift; Sulige gas field; O rdos basin © 1994-2007 China Academic Journal Electronic Publishing House. All rights reserved. http://www.cnki.net
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